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1.- STRATIGRAPHIC EVOLUTION OF LATEST CRETACEOUS TO EARLY TERTIARY DIFUNTA FORELAND BASIN IN NORTHEAST MEXICO; INFLUENCE OF SALT WITHDRAWAL ON TECTONICALLY INDUCED SUBSIDENCE BY THE SIERRA MADRE ORIENTAL FOLD AND THRUST BELT
AMERICAN ASSOCIATION OF PETROLEUM GEOLOGISTS; TULSA, OK; USA; UNITED STATES, 2003
THE CIRCUM-GULF OF MEXICO AND THE CARIBBEAN; HYDROCARBON HABITATS, BASIN FORMATION, AND PLATE TECTONICS
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